Lepidaspis, Dineley & Loeffler, 1976
publication ID |
https://doi.org/ 10.5252/g2013n3a3 |
DOI |
https://doi.org/10.5281/zenodo.5463525 |
persistent identifier |
https://treatment.plazi.org/id/493F87AA-FF92-6224-697E-FDBFFDCAFA34 |
treatment provided by |
Marcus |
scientific name |
Lepidaspis |
status |
|
Lepidaspis ? sp.
( Fig. 6D View FIG )
MATERIAL. — Specimen GIT 580-2: isolated tessera.
LOCALITY AND STRATIGRAPHIC HORIZON. — Same as specimens GIT 580-1, 3, 4, 6 and 7: locality (sample) 73, Tonnel’nyj Brook, south of De Long Strait, Chukotka; Lower Member (1) of Enmakaj Formation, Lochkovian.
DESCRIPTION ħe specimen is a diamond-shaped, 1.7 mm long tessera with a single central, narrow, elongate tubercle (c. 1.4 mm long). ħis tubercle has denticulated edges. Each denticulation is simple (undivided). Additionally, on each side of this central tubercle occurs a much smaller narrow tubercle ( Fig. 6D View FIG ). ħe base of the tessera is perforated by small foramina of the underlying (probably reticulated) layer. ħis tessera compares well with those of Lepidaspis serrata Dineley & Loeffler (1976 : figs 74, 76, pl. 32: 6, 7), and especially with the tessera in their plate 32: 6, which bears a small lateral tubercle beside the main central denticulated one. However, because we have here a single tessera, it is difficult to compare with the great variability of shapes observed on Lepidaspis serrata tesserae ( Dineley & Loeffler 1976), and so only tentatively assign GIT 580-2 to Lepidaspis .
GIT |
Institute of Geology at Tallinn University of Technology |
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